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1TKO

Iron-oxo clusters biomineralizing on protein surfaces. Structural analysis of H.salinarum DpsA in its low and high iron states

Summary for 1TKO
Entry DOI10.2210/pdb1tko/pdb
Related1MOJ 1TJO 1TK6 1TKP
DescriptorIron-rich dpsA-homolog protein, SULFATE ION, FE (III) ION, ... (5 entities in total)
Functional Keywordsdpsa, high iron, iron cluster, metal binding protein
Biological sourceHalobacterium salinarum
Cellular locationCytoplasm : Q9HMP7
Total number of polymer chains4
Total formula weight82847.60
Authors
Zeth, K.,Offermann, S.,Essen, L.O.,Oesterhelt, D. (deposition date: 2004-06-09, release date: 2004-10-19, Last modification date: 2023-08-23)
Primary citationZeth, K.,Offermann, S.,Essen, L.O.,Oesterhelt, D.
Iron-oxo clusters biomineralizing on protein surfaces: structural analysis of Halobacterium salinarum DpsA in its low- and high-iron states.
Proc.Natl.Acad.Sci.USA, 101:13780-13785, 2004
Cited by
PubMed Abstract: The crystal structure of the Dps-like (Dps, DNA-protecting protein during starvation) ferritin protein DpsA from the halophile Halobacterium salinarum was determined with low endogenous iron content at 1.6-A resolution. The mechanism of iron uptake and storage was analyzed in this noncanonical ferritin by three high-resolution structures at successively increasing iron contents. In the high-iron state of the DpsA protein, up to 110 iron atoms were localized in the dodecameric protein complex. For ultimate iron storage, the archaeal ferritin shell comprises iron-binding sites for iron translocation, oxidation, and nucleation. Initial iron-protein interactions occur through acidic residues exposed along the outer surface in proximity to the iron entry pore. This narrow pore permits translocation of ions toward the ferroxidase centers via two discrete steps. Iron oxidation proceeds by transient formation of tri-iron ferroxidase centers. Iron storage by biomineralization inside the ferritin shell occurs at two iron nucleation centers. Here, a single iron atom provides a structural seed for iron-oxide cluster formation. The clusters with up to five iron atoms adopt a geometry that is different from natural biominerals like magnetite but resembles iron clusters so far known only from bioinorganic model compounds.
PubMed: 15365182
DOI: 10.1073/pnas.0401821101
PDB entries with the same primary citation
Experimental method
X-RAY DIFFRACTION (2.9 Å)
Structure validation

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数据于2024-11-13公开中

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